Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Most slopes currently have very weak and fragile facets and depth hoar on or near the ground that formed during the prolonged November dry periods. Recent snow and wind loading have built cohesive slabs on top of these persistent weak layers leading to this poor snowpack structure of strong over weak. These weak layers haven't received much of a break over the last week and will continue to struggle to adjust to the recent load from last night. At lower elevations where slabs are not as thick, you're more likely to get these weak layers to collapse to trigger an avalanche. At upper elevations, weak layers are buried under deeper stiffer slabs and may take you finding that "sweet spot" in likely trigger points near rock outcroppings and on the margins of the slab. These persistent slab avalanches can break widely across the slope or terrain features and could be very large taking with it most of the season's snowpack and most likely would not be survivable. You can trigger one of these large avalanches from a long distance away, so continue to give steep slopes above you wide berths.